Intraannual and interannual changes in the surface area of a closed lake complex in southwestern Siberia using NOAA images

The Lake Chany complex, located in southwestern Siberia, consists of large shallow lakes with an average depth of about 2.2m. The area of the lake fluctuates with the water level, which is closely related to the amount of inflow and evaporation, as the lake complex is endorheic. Using National Ocean...

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Published inLimnology Vol. 7; no. 2; pp. 123 - 128
Main Authors Shikano, Shuichi, Kawano, Koichi, Kudoh, Jun-ichi, Yurlov, Alexander K, Kikuchi, Eisuke
Format Journal Article
LanguageEnglish
Published Tokyo Springer Nature B.V 01.08.2006
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Abstract The Lake Chany complex, located in southwestern Siberia, consists of large shallow lakes with an average depth of about 2.2m. The area of the lake fluctuates with the water level, which is closely related to the amount of inflow and evaporation, as the lake complex is endorheic. Using National Oceanic and Atmospheric Administration (NOAA) satellite images of the ice-free periods from 1999 to 2004, we evaluated the seasonal changes in the lake area and surrounding vegetation of the Lake Chany complex. The maximum lake area was observed in early May and decreased until late July. The lake area in August was about 60% of the maximum. Subsequently, the area tended to increase until early October. Compared to ground-truth data, the areas undergoing seasonal fluctuations in the NOAA images corresponded to vast stands of vegetation (Phragmites australis) that were several kilometers wide. These areas seem to be influenced by the inflow of snow-melt water and reed growth. Although interannual differences in the seasonal change in lake area were not great for the whole lake complex, the isolated Yudinskii Pool showed large interannual differences during summer and autumn, suggesting that monitoring this area using NOAA images will be useful for estimating the interannual fluctuations in the southwestern Siberian environment.[PUBLICATION ABSTRACT]
AbstractList The Lake Chany complex, located in southwestern Siberia, consists of large shallow lakes with an average depth of about 2.2m. The area of the lake fluctuates with the water level, which is closely related to the amount of inflow and evaporation, as the lake complex is endorheic. Using National Oceanic and Atmospheric Administration (NOAA) satellite images of the ice-free periods from 1999 to 2004, we evaluated the seasonal changes in the lake area and surrounding vegetation of the Lake Chany complex. The maximum lake area was observed in early May and decreased until late July. The lake area in August was about 60% of the maximum. Subsequently, the area tended to increase until early October. Compared to ground-truth data, the areas undergoing seasonal fluctuations in the NOAA images corresponded to vast stands of vegetation (Phragmites australis) that were several kilometers wide. These areas seem to be influenced by the inflow of snow-melt water and reed growth. Although interannual differences in the seasonal change in lake area were not great for the whole lake complex, the isolated Yudinskii Pool showed large interannual differences during summer and autumn, suggesting that monitoring this area using NOAA images will be useful for estimating the interannual fluctuations in the southwestern Siberian environment.[PUBLICATION ABSTRACT]
The Lake Chany complex, located in southwestern Siberia, consists of large shallow lakes with an average depth of about 2.2m. The area of the lake fluctuates with the water level, which is closely related to the amount of inflow and evaporation, as the lake complex is endorheic. Using National Oceanic and Atmospheric Administration (NOAA) satellite images of the ice-free periods from 1999 to 2004, we evaluated the seasonal changes in the lake area and surrounding vegetation of the Lake Chany complex. The maximum lake area was observed in early May and decreased until late July. The lake area in August was about 60% of the maximum. Subsequently, the area tended to increase until early October. Compared to ground-truth data, the areas undergoing seasonal fluctuations in the NOAA images corresponded to vast stands of vegetation (Phragmites australis) that were several kilometers wide. These areas seem to be influenced by the inflow of snow-melt water and reed growth. Although interannual differences in the seasonal change in lake area were not great for the whole lake complex, the isolated Yudinskii Pool showed large interannual differences during summer and autumn, suggesting that monitoring this area using NOAA images will be useful for estimating the interannual fluctuations in the southwestern Siberian environment.
Author Shikano, Shuichi
Yurlov, Alexander K
Kikuchi, Eisuke
Kudoh, Jun-ichi
Kawano, Koichi
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CitedBy_id crossref_primary_10_1002_wat2_1227
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crossref_primary_10_15372_RGG2019117
crossref_primary_10_1016_j_jaridenv_2018_09_008
Cites_doi 10.1080/01431168608948944
10.4324/9780203412152
10.1016/0168-1923(93)90031-C
10.1007/BF01093590
10.1109/IGARSS.2003.1295312
10.1002/(SICI)1096-9837(199904)24:4<283::AID-ESP950>3.0.CO;2-9
10.1023/B:HYDR.0000008595.14393.77
10.1029/95JC02125
10.1016/0034-4257(94)90036-1
10.1017/S0376892902000103
10.1007/BF00018787
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Snippet The Lake Chany complex, located in southwestern Siberia, consists of large shallow lakes with an average depth of about 2.2m. The area of the lake fluctuates...
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StartPage 123
SubjectTerms Aquatic plants
Birds
Closed lakes
Evaporation
Fluctuations
Freshwater
Ice-free periods
Meltwater
Snowmelt
Vegetation
Water depth
Water inflow
Water levels
Title Intraannual and interannual changes in the surface area of a closed lake complex in southwestern Siberia using NOAA images
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